Images of Old Hawaiʻi

by Peter T Young 1 Comment

Nāhuku

Nāhuku (the protuberances) is a lava cave, or more commonly called a lava tube.

Lava tubes are natural conduits through which lava travels beneath the surface of a lava flow. Tubes form by the crusting over of lava channels and pāhoehoe flows.  When the supply of lava stops at the end of an eruption or lava is diverted elsewhere, lava in the tube system drains downslope and leaves partially empty conduits beneath the ground.  (USGS)

One of the most photographed lava tubes is Nāhuku in the Hawaiʻi Volcanoes National Park.  It was found in 1913 by Lorrin Andrews Thurston (July 31, 1858 – May 11, 1931,) a local newspaper publisher, a lawyer, politician and businessman.

Thurston was born and raised in the Kingdom of Hawaiʻi, grandson of the first Christian missionaries to Hawaiʻi. He played a prominent role in the overthrow of the Hawaiian Kingdom that replaced Queen Liliʻuokalani with the Republic of Hawaiʻi.

But this story is about a cave in Volcano, not politics.

Thurston first visited Kīlauea in 1879 at the age of 21 with Louis von Tempsky.  Thurston wrote that “we hired horses in Hilo and rode to the volcano, from about eight o’clock in the morning to five in the afternoon.”  (NPS)

Ten years later Thurston’s first mark upon the Volcano landscape appeared. In 1889, using his position as Minister of the Interior, he oversaw the construction of an improved carriage road from Hilo to Volcano.

The road was completed in 1894 allowing four-horse stages to transport visitors from Hilo to Volcano in seven hours. This feat would greatly increase the number of people able to view the volcano at Kīlauea.  (NPS)

The cave/lava tube he later found is also known as Keanakakina (Cave of Thurston – keana meaning cave and kakina the Hawaiian name for Thurston.)

“On Aug. 2nd a large party headed by LA Thurston explored the lava tube in the twin Craters recently discovered by Lorrin Thurston, Jr. Two ladders lashed together gave comparatively easy access to the tube and the whole party, including several ladies, climbed up.”

“No other human beings had been in the tube, as was evidenced by the perfect condition of the numerous stalactites and stalagmites. Dr. Jaggar estimated the length of the tube as slightly over 1900 feet. It runs northeasterly from the crater and at the end pinches down until the floor and roof come together…”  (Thayer, Kempe)

Thurston and George Lycurgus (Uncle George) were instrumental in getting the volcano recognized as Hawaiʻi Volcanoes National Park.  Starting in 1906, the two were working to have the Mauna Loa and Kilauea Volcanoes area so designated.  In 1912, geologist Thomas Augustus Jaggar arrived to investigate and joined their effort.

Jaggar had tried to lead several expeditions to the top of Mauna Loa in 1914 but was unsuccessful due to the elevation (13,678 feet) and the harsh conditions: rough lava, violent winds, noxious fumes, shifting weather, extreme temperatures and a lack of shelter, water and food.  (Takara)

On August 1, 1916, President Woodrow Wilson signed the country’s 13th National Park into existence – Hawaiʻi National Park.  At first, the park consisted of only the summits of Kīlauea and Mauna Loa on Hawaiʻi and Haleakalā on Maui.

Eventually, Kīlauea Caldera was added to the park, followed by the forests of Mauna Loa, the Kaʻū Desert, the rain forest of Olaʻa and the Kalapana archaeological area of the Puna/Kaʻū Historic District.

On, July 1, 1961, Hawaiʻi National Park’s units were separated and re-designated as Haleakalā National Park and Hawaii Volcanoes National Park.

OK, back to Nāhuku.

This 500-year old, 600-foot long (with ceilings between 10 and 30-feet) lava tube is accessed via a short trail down, through and around back to the starting point (overall, it’s about 1/3-mile and takes about 20-30-minutes.)  (The lava tube available for viewing is about 600-feet, the actual tube is approximately 1,500-feet.)

It is one of the very few readily-accessible lava caves/tubes for folks to see in Hawaiʻi.  The cave has two openings used as an entrance/exit for the trail. The primary entrance is reached via a bridge.  The cave/tube is lit with electric lights and has a flat rock floor.

The main entrance of the cave is near the top of the side wall of a closed depression. Its location is close to the margin of the Kilauea Iki section of the present-day Kilauea caldera-crater complex. This closed depression has the Hawaiian name Kaluaiki.  (Halliday)  The other entrance is a ceiling hole, caused by roof collapse much after the cave had cooled.  (Kempe)

Hawaiʻi Volcanoes National Park is worth seeing, and a stop at Nāhuku (Thurston Lava Tube) is worth making, even if you have seen it a million times before.  Enjoy this and other day hikes in the Park.

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Penguin Bank

“As for the depths themselves, the greatest yet discovered … was the Penguin Deep, discovered by the British vessel Penguin (in 1896) north of New Zealand where a depth of 5,155 fathoms was found.”  (New York Tribune, January 25, 1920)  (Four years later, the USS Nero instruments registered a depth of 5,269 fathoms – almost six miles.)

HMS Penguin was an Osprey-class sloop (United Kingdom, later Australia.) Launched on 1876, Penguin was operated by the Royal Navy from 1877 to 1881, then from 1886 to 1889.

She was 170 feet long, had a beam of 36 feet, a draft of 15 feet 9 inches and had a displacement of 1,130 tons.  The propulsion machinery consisted of a single engine that gave her a top speed of 9.9 knots and a maximum range of 1,480 nautical miles (1,700 mi.) (She was also Barque rigged.) The standard ship’s company was 140-strong.

After being converted to a survey vessel, Penguin was recommissioned in 1890, and conducted survey work around the Western Pacific islands, New Zealand and the Great Barrier Reef until 1908, when she was demasted and transferred to the Australian Commonwealth Naval Forces for use as a depot and training ship in Sydney Harbor.

After this force became the Royal Australian Navy, the sloop was commissioned as HMAS Penguin in 1913. Penguin remained in naval service until 1924, when she was sold off and converted into a floating crane. (The vessel survived until 1960, when she was broken up and burnt.)

In addition to finding the deepest bottom of the ocean (at the time, as noted above,) Penguin was involved in finding other ocean bottoms – one happened in Hawaiʻi.

Let’s step back a bit.

Hawaiʻi is the world’s most-isolated populated-place.  In round numbers, we are 5,000-miles from Washington DC, New York, Florida, Australia, Philippines, Hong Kong & the North Pole; 4,000-miles from Chicago, Tokyo, New Zealand & Guam and 2,500-miles from Los Angeles, all other West Coast cities, Samoa, Alaska & Mexico.

While, today, technology keeps us constantly and instantly in touch and aware of world events, the same was not true in the past.  Prior to the beginning of the 20th century, you had at least a one-week time lag in receiving “news” (that arrived via ships.)

At the time, Great Britain and its possessions were spread across the globe.  Communicating between these holdings created challenges.

Step in Sir Sandford Fleming, a Scottish-born Canadian engineer and inventor.  Among other feats, he proposed worldwide standard time zones, designed Canada’s first postage stamp, and, in 1862, Fleming had submitted a plan to the Government for a trans-Canada railway.

In the same year, he was appointed Chief Engineer of the British-Australian Telegraph Company.  Fleming was one of the staunch advocates for a Pacific telegraph cable.

A Colonial Conference held in Sydney in 1877 passed resolutions concerning a Pacific cable, one of which sought subsidies from the US Government for a cable running from the United States to New Zealand.

In 1879, Fleming wrote to the Telegraph and Signal Service in Ottawa about the railway and cable:  “If these connections are made we shall have a complete overland telegraph from the Atlantic to the Pacific coast.”

“It appears to me to follow that, as a question of imperial importance, the British possessions to the west of the Pacific Ocean should be connected by submarine cable with the Canadian line. Great Britain will thus be brought into direct communication with all the greater colonies and dependencies without passing through foreign countries.”

The completion of the Canadian Pacific Railway in 1885, and with it a telegraph line across Canada, strengthened Fleming’s position. The decision to extend the railway to Vancouver in 1886 helped even more.  (atlantic-cable)

At the 1893 Australasian Conference held in Sydney the Postmaster General of New South Wales suggested laying a cable from New Caledonia (already linked to Australia by cable) to Fiji, Honolulu and San Francisco.

That brings us back to the Penguin. She was commissioned to make soundings and survey areas for suitable cable routes and station locations.

That brought her to Hawaiʻi.

“The Penguin left Sydney on April 10, proceeding by way of Suva Fiji to Palmyra Island, where a party was landed to observe the tides.  The steamer then proceeded to the north and made an accurate survey of Kingman reef, which was found to be sixty miles due north of Palmyra Island.  (The Sun (NY,) July 30, 1897)

“The British survey steamer Penguin, which arrived (in Honolulu) yesterday, has just completed the preliminary survey for the Australian-British Columbian cable. She ran a line of soundings from Palmyra Island to a point 300-miles to the southward of Honolulu, finding and average depth of 2,700 fathoms.”

“After spending three weeks here in receiving general repairs the Penguin will return to Palmyra Island and run a line of soundings southwest to Sydney.”  (The Sun (NY,) July 30, 1897)

The Penguin made another discovery here.

“The Penguin … must await stores and advices before resuming her survey work, but in the interim will make an accurate survey of the shoal discovered to the southward, sailing from here on the 12th for that purpose, and returning again later.”  (The Hawaiian Star, August 7, 1897)

“HBMS Penguin will leave at daylight tomorrow to survey a shoal near this group, expecting to be back Sunday morning.”  (Evening Bulletin, August 11, 1897)

“Although the officers aboard the Penguin were loathe to give any information it was learned that at about 10 o’clock on Tuesday night (July 20, 1897) and while about 30-miles of the Island of Oʻahu, the ‘tell-tale’ of the ship showed that a shoal 26-fathoms below the surface of the water, had been struck.”  (Pacific Commercial, July 22, 1897; Clark)

The name of the shoal appears to have varied early names.

“The steamer JA Cummins went off fishing with a party of excursionists this morning.  The steamer will cruise about Kamehameha shoal (the new reef discovered by HBMS Penguin) and return tonight or early tomorrow.”  (Evening Bulletin, September 11, 1897)

“The Albatross started from Honolulu on July 9.  She first went dredging at the Penguin shoal and went from there to Puako, on Hawaii.”  (Evening Bulletin, July 29, 1902)

Today, it’s more commonly referred to as Penguin Bank.

Penguin Bank (about 20 miles long and 10 miles wide within the Kaiwi Channel) is the eroded summit of a sunken volcano, now a broad submarine shelf off Molokai Island with depths of less than 200 feet deep. It is capped with sand and fossil corals. The Bank is generally too deep for most live corals and is a relatively barren habitat compared to shallower waters nearby. The base rock is lava of the same kind that forms Molokai Island.  (Grays Harbor)

It was one of the seven principal volcanoes (along with West Molokai, East Molokai, Lānai, West Maui, East Maui and Kahoʻolawe) that formerly constituted of Maui Nui.

The top of Penguin Bank and other banks and shelves throughout the Pacific basin are found at similar depths, because these banks were formed by an interplay between reef growth and past low stands of global sea level.  (Agegian)

Penguin Bank is noted for highest concentrations of humpback whales during their winter sojourns in Hawaiʻi. While in Hawaiʻi, Humpback Whales are found in shallow coastal waters, usually less than 300-feet. The average water depth in Penguin Banks is around 200-feet, but water depths can range from about 150-feet to 600-feet.  (NOAA)

It’s also one of Hawaiʻi’s premier fishing sites.  “Yachts May Cruise – The yachtsmen are thinking of making a cruise starting Saturday and returning Monday night, Monday being Labor Day.”

“Two plans are at present being discussed.  One is to go to Waianae and remain off that place fishing.  The other plan is a more extensive on.  It is to go to Penguin Shoal on the west coast of Molokai to fish, returning Monday via Rabbit Island, where the yachtsmen may stop for a day’s rabbit and bird shooting.”  (Evening Bulletin, September 1, 1904)

In 1902, the first submarine cable across the Pacific was completed (landing in Waikīkī at Sans Souci Beach) linking the US mainland to Hawaiʻi, Canada, Australia, New Zealand and Fiji and Guam to the Philippines in 1903.   (The first Atlantic submarine cable, connecting Europe with the USA, was completed in 1866.)

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Pāhonu

Honu neʻe pū ka ʻāina
The land moves like the turtle.
(Land passes slowly but inexorably from owner to heir.)
(Pukui)

From its earliest period of occupation, the Waimānalo Bay region was an extensive agricultural area, featuring taro farms that used the traditional Hawaiian loʻi (pondfield) cultivation system.

Taro was grown in the lowlands, irrigated with water from Waimānalo Stream, as well as on terraced sections that were watered by the small streams and springs flowing out of the Koʻolau Range.

These terraced sections extended for nearly 2-miles in a semicircle at the foot of the mountains around the broad base of the Waimānalo valley. By the 1850s, the area’s fertile soil provided not only taro but also breadfruit, mountain apple, kukui and coconut trees, sweet potatoes and sugar cane.  (NPS)

In addition to the agrarian-based economy, several fishing villages dotted the bay’s shoreline. Two of the best-known villages in the area were Kaupō and Kukui. Kaupō was on a small peninsula opposite Mānana Island (Rabbit Island) and just northwest of Makapuʻu Beach Park (where Sea Life Park is located.)

The village may have been depopulated during the early-1800s and probably was repopulated during the early-1850s when a disastrous smallpox epidemic struck Honolulu and Hawaiians settled temporarily in the Waimānalo Bay region to escape its ravages.

The small fishing village of Kukui was further northwest, along the bay in the Kaiona Beach vicinity near Pāhonu Pond (‘Turtle enclosure’) – a prehistoric walled enclosure where it is said that turtles were kept for the use of Hawaiian chieftains.  (NPS)

Before we go there, let’s look at some findings of Dr Marion Kelly where she speaks of three main technological advances resulting in food production intensification in pre-contact Hawai‘i: (a) walled fishponds, (b) terraced pondfields with their irrigation systems and (c) systematic dry-land field cultivation organized by vegetation zones.

The Hawaiian walled fishpond stands as a technological achievement unmatched elsewhere in island Oceania.  Hawaiians built rock-walled enclosures in near shore waters, to raise fish for their communities and families.  It is believed these were first built around the fifteenth-century.

The general term for a fishpond is loko (pond), or more specifically, loko iʻa (fishpond).  Loko iʻa were used for the fattening and storing of fish for food and also as a source for kapu (forbidden) fish.

Samuel Kamakau points out that “one can see that they were built as government projects by chiefs, for it was a very big task to build one, (and) commoners could not have done it (singly, or without co-ordination.)” Chiefs had the power to command a labor force large enough to transport the tons of rock required and to construct such great walls.

The fishponds just described refer to aquaculture to grow fish – they were found throughout the Islands; however, at Waimānalo, Oʻahu, the only remaining aquaculture of green sea turtle known to have been carried out by the early-Hawaiians involved a coastal pond named Pāhonu that was used to maintain turtles until they were ready to be eaten.  (NOAA)

The green sea turtle is the principal marine turtle species in the Hawaiian Islands.  Common names used in the Hawaiian Archipelago include honu, green turtle and green sea turtle.  They are herbivorous, feeding primarily on seagrasses and algae. This diet is thought to give them greenish-colored fat, from which they take their name. (NOAA)

In Hawaiʻi, as throughout Polynesia and other islands in the pacific, sea turtles have always been a traditional part of the local culture and have historically been revered as special and sacred beings.  (Luna)

“There was once a chief who was so fond of turtle meat that he ordered a sea wall be built to keep captured turtles from escaping.  Every turtle caught by a fisherman was put into this enclosure.  No one else was allowed to partake of turtle meat under penalty of death.  No one dared to eat turtle as long as the old chief lived.”  (Pukui; Maly)

Kikuchi in his “Hawaiian Aquaculture Systems,” notes that “An early visitor to Waikiki area remarked that the ruling chief of Oʻahu, Kahekili, ‘mentioned also some others where he had a quantity of turtle.’”

“… We walked back to Mr. Castle’s house, where we sat on a long bench outside, facing the sea.  There Aiona told me the story of Pa-honu, an enclosure for turtles that was once located back of Mrs. Wall’s present home.”  (Pukui; Maly)

Pāhonu, the offshore pond (500 feet long, 50 feet wide,) is just south of Kaiona Beach Park fronting the shoreline; a line of stones, submerged at high tide, but visible at low tide, notes its location.  (Pukui)

Kaiona Beach Park, a small four-acre park at the south end of Waimānalo Bay, is a popular camping site that has also been used for many years as a community boat anchorage.

In 1998, residents of Waimānalo built a boat ramp in the south end of the park, the only paved ramp in Waimānalo. They also placed a monument to Hawaiian fishers from their community near the ramp. Kaiona means “attractive sea.  (Clark)

The beachfront residence named Pāhonu inland of the pond was used from 1980 to 1988 as the base of operations for the popular television series, Magnum PI.  A surf site borders a small channel through the reef and is also known as Magnums. (Ulukau) The ‘Magnum’ house has been removed and other houses are it its place.
 
Next to Pāhonu is Kaʻakaupapa (shallows at the right.)  The old saying of this place was, “Papa ke kānaka, papa nā mea a pau”—“Multitudes of people, multitudes of gods, all in multitudes.”  (Aiona, Informant, Sept. 14, 1939; Cultural Surveys)

Nearby is the Shriners Club, a private clubhouse that opened on April 20, 1931. Popularly known as Shriners Beach, it is used for a wide variety of events, including wedding receptions, birthday parties and other social gatherings.  (Clark)

The green turtle is listed as endangered by the International Union for the Conservation of Nature. In 1978, the Hawaiian population of the green turtle was listed as threatened under the U.S. Endangered Species Act of 1973.  NOAA Fisheries and the U.S. Fish and Wildlife Service (USFWS) have joint jurisdiction for green sea turtles.

State and Federal laws prohibit harassing, harming, killing, or keeping sea turtles in captivity without a permit allowing these activities for research or educational purposes. Divers should be aware that riding turtles is illegal and puts these animals under stress.

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Kaumālapaʻu

The total land area of Lānai is 89,305 acres, divided into 13 ahupua‘a (traditional land divisions.)  In the traditional system, respective konohiki served as land managers over each. These konohiki were subject to control by the ruling chiefs.

At the time of the Great Māhele (1848,) lands on Lānai were divided between lands claimed by King Kamehameha III (Kauikeaouli) (40,665 acres,) which were known as the Crown Lands, and the lands to be claimed by the chiefs and people (48,640 acres,) which were called the Government Lands.

By 1907, more than half the island of Lānai was in the hands of native Hawaiians. Just 14 years later, in 1921, only 208.25 acres of land remained in native Hawaiian ownership. By 1875 Walter Gibson had control, either through lease or direct ownership, of nine‐tenths of Lānai’s lands. (Lānai Community Plan)

When James Dole bought Lānai, ranching was a thriving business under the control of George Munro. Shortly after the purchase, Dole got Munro working at removing cattle from potential pineapple lands. As soon as cattle were fattened they were sold. Ranching operations became a secondary priority to pineapple development.

During 1923, the company embarked on making major improvements to the island of Lānai.  At first, Dole wanted to name the town Pine City, but the post office department objected because there were too many “pine” post offices in the mainland United States.  So the plantation town was called Lānai City.

Dole hired Mr. Root, an engineer, to lay out and plan the town. Root arrived at Mānele Bay to begin his work. He designed the central park with a symmetrical grid of residential streets, which remains the configuration of Lānai City today.” (Lānai Community Plan)

Between 1922 and 1992, pineapple plantation operations provided the people of Lānai with a way of life.  James Doles’ Hawaiian Pineapple Company evolved and many of the innovations in cultivation, equipment design, harvesting, irrigation and labor relations developed on the Lānai plantation, and came to be used around the world. (Lānai Culture & Heritage Center)

Mānele Bay was the main port of entry for Lānai; its primary purpose was to ship pineapple off the island. On the eastern side of the island, remnants of Halepalaoa Landing can be seen; this was used primarily to ship cattle. It’s also reported that in the late 1800s, a steamer landing was located on the western shore of Lānai Island and served as a docking grounds.

A new harbor was needed.  In 1923 to 1926, Kaumālapaʻu Bay, a natural, sheltered cove on the southwest side of Lānai, was developed into the main shipping harbor from which pineapple and all major supplies for Lānai were shipped and received.

“… we learned that the breakwater is composed of 116,000-tons of rock blasted from the cliffs and dropped into the water.  The Kaumalapau harbor entrance is 65-feet deep, and the minimum depth of the harbor is 27-feet.  The wharf is 400-feet long and the boat landing is 80-feet in length.”  (Lanai “The Pineapple Kingdom, 1926)

Bins filled with pineapple were unloaded from the trucks (steam cranes were still used through the 1960s), and placed on the barges for shipping to the cannery at Iwilei, Honolulu, Oʻahu. Tug boats were used to haul the barges – empty bins and supplies to Lānai, and filled pineapple bins to the cannery.

Because of the demands of work at Kaumālapaʻu, Lānai’s “second city” was developed, and known as “Harbor Camp.” The Harbor Camp included around 20 homes and support buildings, and sat perched on the cliffs above Kaumālapaʻu Bay.  (Lānai Culture & Heritage Center)

Surmising from the vast archaeological features on the cliffs above Kaumālapaʻu Gulch, Kaumālapaʻu Harbor was probably a very important settlement (seasonal and/or permanent) for native Hawaiians. (Social Research Pacific)

Access to fishing, whether by boat or off the shoreline, is easily attained at Kaumālapaʻu.  One of the sites immediately mauka of the harbor is called “Fisherman’s Trail.” In the 1862 letter requesting settlement and use of Lānai, even Gibson indicated the importance of fishing as the primary source of subsistence for the island’s inhabitants.

The village of Kaunolu, just to the south of Kaumālapaʻu was known as a “fishing village”. Given its proximity to Kaumālapaʻu, it is highly likely that neighboring Kaumālapaʻu also offered good fishing grounds to Hawaiians. The Kaumālapaʻu Trail extends from Lānai City down to Kaumālapaʻu.   (Social Research Pacific)

In the Māhele, the ahupuaʻa of Kamoku and Kalulu (which adjoin the existing Kaumālapaʻu Harbor) were retained by the King (Kamehameha III), though the ‘ili of Kaumālapaʻu 1 & 2 were given by the King to the Government.

The Kaumālapaʻu Harbor breakwater was in disrepair for many years following several hurricanes and seasonal storms.  Completed in 2007, 40,000-tons of new stone was added to the reshaped breakwater, 800 concrete Core-Locs (each weighing 35 tons) were put in place and a 5-foot- thick concrete cap was cast on top of the breakwater to complete the project.  (Traylor)

Today, as in the early 1920s, Kaumālapaʻu Harbor is the main commercial seaport and Lānai’s lifeline to the outside world, with Young Brothers’ barge and other commercial activity in and out of Lānai.

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Pāpōhaku

A chief from east Molokai and a few of his people boarded canoes and set off around the island. They found themselves on the southwest coast of Molokai.  They paddled up to some fishermen who had a large catch of opelu. Hungry, they began to eat.

As they were all eating with great satisfaction, another group of fishermen came by and cried: “Stop. Do not eat the opelu. This is the season of opelu kapu.” However, the visiting chief only had a kapu for eating turtle, so they continued eating.

The fishermen attacked the visiting chief and his men. Overpowered, they were brought before the kahuna. The visiting chief became very ill, and the only way to make things right was a human sacrifice to save the chief from death. One of his men offered himself as a sacrifice and the chief recovered.

The kahuna ordered a tree planted on the grave of the willing victim. The grave was on shore; when the tide was high, the waves would wash sand from the grave. Thus, in a very short time, the body would be exposed.

In respect and remembrance, the chief ordered his men to build a stone wall.  The chief himself put the last stone on the wall, saying as he did so, “I call this place Pāpōhaku, ‘Stone Wall.’” (DLNR)

Today, the sandy beach is seen as the primary feature here (it’s over 2-miles long and 300-feet wide, the largest on the island and one of the largest in the Islands.)  It lies between two headlands, Puʻu Koaʻe to the south and Puʻu o Kaiaka to the north.

The sand caught people’s attention.

First, folks looked to replenish eroding beaches by harvesting sand from one area and filled in at another (primarily at Waikīkī.)  Reports from the 1920s and 1930s reveal that sand was brought to Waikīkī Beach, via ship and barge, from Manhattan Beach, California.

As the Manhattan Beach community was developing, it found that excess sand in the beach dunes and it was getting in the way of development there.  At the same time, folks in Hawai‘i were in need for sand to cover the rock and coral beach at Waikīkī.

Later, Waikīkī’s sand was trucked from various points around Hawai‘i including O‘ahu’s North Shore – in particular, Waimea Bay Beach, a sand bar off the town of Kahuku and Pāpōhaku Beach on Molokai.

Reportedly, before sand mining operations removed over 200,000 tons of sand at Waimea Bay to fill beaches in Waikīkī and elsewhere, there was so much sand that if you would have tried to jump off Pōhaku Lele, Jump Rock, you would have jumped about six feet down into the sand below.

Then came statehood, and the building boom of the following decades.

“Increased use of concrete by building contractors resulted in more output of sand required for blending with crushed basalt fines used in concrete aggregate.  A substantial gain was noted in the use of coral dune sands from the north shores of Oʻahu Island.  By yearend, Honolulu Construction & Draying Co Ltd (HC&D) was prepared to barge sand from Molokai Island to supply some of Oahu’s requirements for the critical material.”  (Minerals Yearbook, 1959)

(HC&D was formed in 1908 by a quarry owner, three construction men and a retired sea captain. The base of the business was the draying (hauling) of construction materials by horse-drawn wagons. In late-1967, HC&D became a wholly owned subsidiary of American Pipe and Construction Co of Monterey Park, California (now it’s known as Ameron Inc.))

In the 1950s, a harbor was dredged and a wharf constructed at Hale O Lono by B&C (Brown and Clewitt) Trucking to ship out sand from Pāpōhaku (B&C also owned Seaside Inn and Pau Hana Inn.) A 1957 contract between Molokai Ranch and HC&D allowed for sand to be removed from a 297-acre southern parcel of Pāpōhaku Beach.

“Sand and gravel was produced at 16 principal beach, dune, and stream deposits. The largest operation was the Molokai sand facility of HC&D Ltd, Hawaiʻi’s major producer, consumer, and supplier of sand, cinder, and crushed stone.”  (Minerals Yearbook, 1964)

“Some of the land out on the western tip of the island is leased to Honolulu Construction and Draying Company Ltd, which mines something like 200,000-yards of sand a year from Pāpōhaku Beach for shipment to Oahu for use in making concrete.”  (Away From It All)

“All day long, every day, had trucks going back and forth from Pāpōhaku to Hale O Lono.”  From the early 1960s to 1975, this massive cache of sand was the site of the largest sand-mining operation in the state.

Some of the sand was drawn from below the high water mark, which was public land and required a government permit; at times the dredge bucket even drew the sand out of the ocean.

This was not legal and HC&D was caught and reportedly fined, resulting in a million-dollar settlement.  In lieu of payment of the fine, reportedly, Molokai Ranch gave the land at Ala Mālama in Kaunakakai.

Even with the decades of sand removal, Pāpōhaku Beach remains one of the longest white sand beaches, and the Pāpōhaku Dune system associated with the beach is among the largest in Islands.

Pāpōhaku Dune (like other sand dunes) is the first and last line of defense against coastal erosion and episodic high waves for the existing structures located behind it.

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